Two Sites in East Asia Add to Spatiotemporal Heterogeneity of Wildfire Activity Across the Paleocene–Eocene Thermal Maximum
Abstract The Paleocene–Eocene Thermal Maximum (PETM; ∼56 Ma) was a period of extreme global warming associated with a massive influx of isotopically light carbon into the ocean–atmosphere system. The burning of Paleocene peatland (wildfire hypothesis) has been proposed as a potential light carbon so...
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| Hoofdauteurs: | , , , , , , , , |
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| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Wiley
2025-01-01
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| Reeks: | Geophysical Research Letters |
| Onderwerpen: | |
| Online toegang: | https://doi.org/10.1029/2024GL113829 |
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